Climate Dynamics

, Volume 37, Issue 1, pp 35–51

Multiproxy summer and winter surface air temperature field reconstructions for southern South America covering the past centuries

  • R. Neukom
  • J. Luterbacher
  • R. Villalba
  • M. Küttel
  • D. Frank
  • P. D. Jones
  • M. Grosjean
  • H. Wanner
  • J.-C. Aravena
  • D. E. Black
  • D. A. Christie
  • R. D’Arrigo
  • A. Lara
  • M. Morales
  • C. Soliz-Gamboa
  • A. Srur
  • R. Urrutia
  • L. von Gunten
Article

DOI: 10.1007/s00382-010-0793-3

Cite this article as:
Neukom, R., Luterbacher, J., Villalba, R. et al. Clim Dyn (2011) 37: 35. doi:10.1007/s00382-010-0793-3

Abstract

We statistically reconstruct austral summer (winter) surface air temperature fields back to ad 900 (1706) using 22 (20) annually resolved predictors from natural and human archives from southern South America (SSA). This represents the first regional-scale climate field reconstruction for parts of the Southern Hemisphere at this high temporal resolution. We apply three different reconstruction techniques: multivariate principal component regression, composite plus scaling, and regularized expectation maximization. There is generally good agreement between the results of the three methods on interannual and decadal timescales. The field reconstructions allow us to describe differences and similarities in the temperature evolution of different sub-regions of SSA. The reconstructed SSA mean summer temperatures between 900 and 1350 are mostly above the 1901–1995 climatology. After 1350, we reconstruct a sharp transition to colder conditions, which last until approximately 1700. The summers in the eighteenth century are relatively warm with a subsequent cold relapse peaking around 1850. In the twentieth century, summer temperatures reach conditions similar to earlier warm periods. The winter temperatures in the eighteenth and nineteenth centuries were mostly below the twentieth century average. The uncertainties of our reconstructions are generally largest in the eastern lowlands of SSA, where the coverage with proxy data is poorest. Verifications with independent summer temperature proxies and instrumental measurements suggest that the interannual and multi-decadal variations of SSA temperatures are well captured by our reconstructions. This new dataset can be used for data/model comparison and data assimilation as well as for detection and attribution studies at sub-continental scales.

Keywords

Climate changeClimate field reconstructionsTemperatureSouth America

Supplementary material

382_2010_793_MOESM1_ESM.pdf (1.6 mb)
Supplementary material 1 (PDF 1674 kb)

Copyright information

© Springer-Verlag 2010

Authors and Affiliations

  • R. Neukom
    • 1
    • 2
  • J. Luterbacher
    • 3
  • R. Villalba
    • 4
  • M. Küttel
    • 1
    • 2
    • 5
  • D. Frank
    • 6
  • P. D. Jones
    • 7
  • M. Grosjean
    • 1
    • 2
  • H. Wanner
    • 1
    • 2
  • J.-C. Aravena
    • 8
  • D. E. Black
    • 9
  • D. A. Christie
    • 10
  • R. D’Arrigo
    • 11
  • A. Lara
    • 10
    • 12
  • M. Morales
    • 4
  • C. Soliz-Gamboa
    • 13
  • A. Srur
    • 4
  • R. Urrutia
    • 10
  • L. von Gunten
    • 1
    • 2
    • 14
  1. 1.Oeschger Centre for Climate Change Research (OCCR)University of BernBernSwitzerland
  2. 2.Institute of Geography, Climatology and MeteorologyUniversity of BernBernSwitzerland
  3. 3.Department of Geography; Climatology, Climate Dynamics and Climate ChangeJustus Liebig University of GiessenGiessenGermany
  4. 4.Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA)CONICETMendozaArgentina
  5. 5.Department of Earth and Space SciencesUniversity of WashingtonSeattleUSA
  6. 6.Swiss Federal Research Institute WSLBirmensdorfSwitzerland
  7. 7.Climatic Research Unit, School of Environmental SciencesUniversity of East AngliaNorwichUK
  8. 8.Centro de Estudios Cuaternarios de Fuego Patagonia y Antártica (CEQUA)Punta ArenasChile
  9. 9.School of Marine and Atmospheric SciencesStony Brook UniversityStony BrookUSA
  10. 10.Laboratorio de Dendrocronología, Facultad de Ciencias Forestales y Recursos NaturalesUniversidad Austral de Chile ValdiviaValdiviaChile
  11. 11.Tree-Ring Laboratory, Lamont-Doherty Earth ObservatoryEarth Institute at Columbia UniversityPalisadesUSA
  12. 12.Núcleo Científico Milenio FORECOS, Fundación FORECOSValdiviaChile
  13. 13.Section of Ecology and Biodiversity, Faculty of Science, Institute of Environmental BiologyUtrecht UniversityUtrechtThe Netherlands
  14. 14.Department of Geosciences, Climate System Research CenterUniversity of MassachusettsAmherstUSA